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Correlation between the mineral and microelement compositions of bottom sediments from the Sea of Okhotsk

  • Proceedings of the 20th National Conference on the Use of Synchrotron Radiation “SR-2014” and the National Youth Conference “Using Synchrotron Radiation”
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Bulletin of the Russian Academy of Sciences: Physics Aims and scope

Abstract

X-ray diffraction, X-ray fluorescence analysis with synchrotron radiation, and vibrational spectroscopy are used to analyze the microelemental composition and minerals that make up the bottom Fe-Mn crusts and sediments from a deep sea borehole in the Deryugin basin, and from the region of the Amur River’s flower water into the Sea of Okhotsk. A correlation between the mineral and microelemental composition, structural characteristics, properties, and sedimentation conditions is established.

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Authors and Affiliations

  1. Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, 630090, Russia

    N. A. Palchik, T. N. Moroz, T. N. Grigorieva, A. V. Darin & L. V. Miroshnichenko

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  1. N. A. Palchik
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  2. T. N. Moroz
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  3. T. N. Grigorieva
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  4. A. V. Darin
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  5. L. V. Miroshnichenko
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Correspondence to N. A. Palchik.

Additional information

Original Russian Text © N.A. Palchik, T.N. Moroz, T.N. Grigorieva, A.V. Darin, L.V. Miroshnichenko, 2015, published in Izvestiya Rossiiskoi Akademii Nauk. Seriya Fizicheskaya, 2015, Vol. 79, No. 1, pp. 111–115.

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Palchik, N.A., Moroz, T.N., Grigorieva, T.N. et al. Correlation between the mineral and microelement compositions of bottom sediments from the Sea of Okhotsk. Bull. Russ. Acad. Sci. Phys. 79, 98–102 (2015). https://doi.org/10.3103/S1062873815010244

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  • DOI: https://doi.org/10.3103/S1062873815010244

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